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Plant Physiol, June 2000, Vol. 123, pp. 671-680

Variation in the Oxygen Isotope Ratio of Phloem Sap Sucrose from Castor Bean. Evidence in Support of the Péclet Effect1

Margaret M. Barbour, Ulrich Schurr, Beverley K. Henry,2 S. Chin Wong, and Graham D. Farquhar*

Environmental Biology Group, Research School of Biological Sciences, Institute of Advanced Studies, Australian National University, G.P.O. Box 475, Australian Capital Territory 2601, Australia (M.M.B., U.S., B.K.H., S.C.W., G.D.F.); and Botanical Institute, University Heidelberg, Im Neuenheimer Feld 360, 69120 Heidelberg, Germany (U.S.)

Theory suggests that the level of enrichment of 18O above source water in plant organic material (Delta ) may provide an integrative indicator of control of water loss. However, there are still gaps in our understanding of the processes affecting Delta . One such gap is the observed discrepancy between modeled enrichment of water at the sites of evaporation within the leaf and measured enrichment of the leaf water as a whole (Delta L). Farquhar and Lloyd (1993) suggested that this may be caused by a Péclet effect. It is also unclear whether organic material formed in the leaf reflects enrichment of water at the sites of evaporation within the leaf or Delta L. To investigate this question castor bean (Ricinus communis L.) leaves, still attached to the plant, were sealed into a controlled-environment gas exchange chamber and subjected to a step change in leaf-to-air vapor pressure difference. Sucrose was collected from a cut on the petiole of the leaf in the chamber under equilibrium conditions and every hour for 6 h after the change in leaf-to-air vapor pressure difference. Oxygen isotope composition of sucrose in the phloem sap (Delta suc) reflected modeled Delta L. A model is presented describing Delta suc at isotopic steady state, and accounts for 96% of variation in measured Delta suc. The data strongly support the Péclet effect theory.


1 This work was supported by Micromass UK Ltd. and by the Australian National University with a visiting fellowship to the Research School of Biological Sciences (to U.S.).

2 Present address: Queensland Department of Natural Resources, 80 Meiers Road, Indooroopilly, QLD 4068, Australia.

* Corresponding author; e-mail farquhar{at}rsbs.anu.edu.au; fax 61-2-6249-4919.

© 2000 American Society of Plant Physiologists



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